FN Archimer Export Format
PT J
TI Stratigraphic simulations of the shelf of the Gulf of Lions: testing subsidence rates and sea-level curves during the Pliocene and Quaternary
BT 
AF LEROUX, Estelle
   RABINEAU, Marina
   ASLANIAN, Daniel
   GRANJEON, Didier
   DROZ, Laurence
   GORINI, Christian
AS 1:1,2;2:1;3:2;4:3;5:1;6:4;
FF 1:;2:;3:PDG-REM-GM-LGG;4:;5:;6:;
C1 UBO, CNRS, IUEM, UMR6538,Domaines Ocean, F-29280 Plouzane, France.
   IFREMER, Ctr Brest, GM, F-29280 Plouzane, France.
   IFP Energies Nouvelles, F-92852 Rueil Malmaison, France.
   Univ Paris 06, UMR 7193, ISTEP, F-75005 Paris, France.
C2 UBO, FRANCE
   IFREMER, FRANCE
   IFP, FRANCE
   UNIV PARIS 06, FRANCE
   CNRS, FRANCE
SI BREST
   AUTRE
SE PDG-REM-GM-LGG
   PDG-REM-GM-LES
   AUTRE
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 2.639
TC 24
UR https://archimer.ifremer.fr/doc/00173/28384/26752.pdf
LA English
DT Article
CR AM-MED-1
   SARDINIA
BO Le Suroît
   L'Atalante
AB Determining the relative importance of factors interacting to control stratigraphic organization is a key issue in sedimentology. The Pliocene-Quaternary chronostratigraphy on the Gulf of Lions platform is still poorly constrained, giving rise to different interpretations of the evolution of its subsidence through time. This paper examines the Pliocene-Quaternary sedimentary filling of the Gulf of Lion's shelf with Dionisos, a numerical stratigraphic model. Our results show that a constant subsidence rate accurately reproduces the observed geometries, whereas a varying subsidence rate reproduces them only if the acceleration of subsidence is limited. At this time-scale, a third-order eustatic curve is also reappraised: a higher resolution curve (built using δ18O measurements) gives a more realistic restitution of our stratigraphic markers. Finally, the constant subsidence rate and sediment fluxes implied in these modellings are discussed relative to climate and local factors of sedimentation
PY 2014
PD JUL
SO Terra Nova
SN 0954-4879
PU Wiley-blackwell
VL 26
IS 3
UT 000334506200009
BP 230
EP 238
DI 10.1111/ter.12091
ID 28384
ER

EF